Zobrazeno 1 - 10
of 153
pro vyhledávání: '"Kulyanitsa, A."'
Autor:
Kulyanitsa, A. L.1 (AUTHOR), Rukhovich, D. I.2 (AUTHOR) landmap@yandex.ru, Koroleva, P. V.2 (AUTHOR), Vilchevskaya, Ye. V.2 (AUTHOR), Kalinina, N. V.2 (AUTHOR)
Publikováno v:
Eurasian Soil Science. 2020, Vol. 53 Issue 12, p1709-1725. 17p.
Autor:
Rukhovich, Dmitry1, Kulyanitsa, Andrey2, Rukhovich, Alexey3, Koroleva, Polina1, Vilchevskaya, Ekaterina1
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM. 2020, p421-428. 8p.
Autor:
Kulyanitsa, A.1, Rukhovich, A.2, Rukhovich, D.2,3 landmap@yandex.ru, Koroleva, P.3, Simakova, M.3
Publikováno v:
Eurasian Soil Science. Apr2017, Vol. 50 Issue 4, p387-395. 9p.
Publikováno v:
Eurasian Soil Science. 53:1709-1725
Large-scale soil maps produced by research institutes for land management (GIPROZEM) are the main source of soil information on arable land in Russia. These maps date back to the 1960s–1990s. During the time that has passed since the last round of
Autor:
Khitrov, Nikolay B., Rukhovich, Dmitry I., Koroleva, Polina V., Kalinina, Natalia V., Trubnikov, Alexey V., Petukhov, Dmitry A., Kulyanitsa, Andrey L.
Publikováno v:
Archives of Agronomy & Soil Science; Dec2020, Vol. 66 Issue 14, p1963-1975, 13p
Autor:
D. I. Rukhovich, N. V. Kalinina, Alexey V. Trubnikov, A. L. Kulyanitsa, P. V. Koroleva, Dmitry A. Petukhov, N. B. Khitrov
Publikováno v:
Archives of Agronomy and Soil Science. 66:1963-1975
The maps of stable intra-field heterogeneity of soil cover were created based on big satellite (remote sensing) data using the technology of the spectral neighbourhood of the soil line. The maps we...
Autor:
D. I. Rukhovich, N. V. Kalinina, A. V. Trubnikov, A. L. Kulyanitsa, D. D. Rukhovich, A. D. Rukhovich, M. S. Simakova, P. V. Koroleva
Publikováno v:
Eurasian Soil Science. 51:1021-1033
A classical soil line (SL) in the RED–NIR spectral space is specified by two coefficients “a” and “b.” In this form, it does not characterize soil types and subtypes. A multitemporal soil line (MSL) represents the major axis of the ellipse
Autor:
D. D. Rukhovich, D. I. Rukhovich, A. D. Rukhovich, M. S. Simakova, P. V. Koroleva, A. L. Kulyanitsa
Publikováno v:
Eurasian Soil Science. 51:345-358
The technique of separation of the spectral neighborhood of soil line (SNSL) makes it possible to perform quantitative estimates of the intensity of agricultural land use. This is achieved via calculation of the frequency of occurrence of bare soil s
Autor:
M. S. Simakova, D. I. Rukhovich, N. V. Kalinina, D. D. Rukhovich, A. L. Kulyanitsa, A. D. Rukhovich, A. V. Trubnikov, P. V. Koroleva
Publikováno v:
Eurasian Soil Science. 50:1375-1385
Soil as a separate natural body occupies certain area with its own set of spectral characteristics within the RED–NIR spectral space. This is an ellipse-shaped area, and its semi-major axis is the soil line for a satellite image. The spectral area
Autor:
D. I. Rukhovich, A. L. Kulyanitsa, P. V. Koroleva, M. S. Simakova, D. D. Rukhovich, A. D. Rukhovich
Publikováno v:
Eurasian Soil Science. 50:387-395
The concept of soil line can be to describe the temporal distribution of spectral characteristics of the bare soil surface. In this case, the soil line can be referred to as the multi-temporal soil line, or simply temporal soil line (TSL). In order t